Small granitic intrusions occur in the progressive metamorphic belts of the Chinese Ahai orogen. SHRIMP U-Pb analyses were performed on zircons separated from a tonalite intrusion and yielded a concordant age of 409.6...Small granitic intrusions occur in the progressive metamorphic belts of the Chinese Ahai orogen. SHRIMP U-Pb analyses were performed on zircons separated from a tonalite intrusion and yielded a concordant age of 409.6±3.7 Ma （ MSWD = 0.93 ）, restricting the emplacement and crystallization of the tonalite intru- sion to the Early Devonian. Combined with the existing geological data of the contemporary large granitic plutons in the Chinese Altai orogen, the tonalite is considered to be formed together with other granitic rocks in a continental arc setting. The tonalite intrusion has consistent foliation with its country rocks, indicating the strain resuiting in the regional deformation should be very strong during or after the early Devonian.展开更多
Jadeite quartzite, essentially a two-phase rock made up of jadeite and quartz, is one of the most important UHP lithologies occur- ring in the Dabie Mountain ultrahigh pressure metamorphic belt and forms layers in bio...Jadeite quartzite, essentially a two-phase rock made up of jadeite and quartz, is one of the most important UHP lithologies occur- ring in the Dabie Mountain ultrahigh pressure metamorphic belt and forms layers in biotite-plagioclase gneiss. High pressure- high temperature studies on natural albite from the country rock gneiss were undertaken to reveal the--in parts----complex mineralogical changes that occur in the jadeite quartzite during prograde metamorphism. Experiments were conducted at 800- 1200~C, in the pressure range of 2.0-3.5 GPa. One of the most intriguing results shows that the low pressure boundary of the jadeite＋coesite stability field is located between about 3.2 GPa at 1000~C and 3.4 GPa at 1200~C, thus about （0.2-0.3）_＋0.1 GPa higher than the quartz-coesite transition curve, given the uncertainty in the present study. Minor amounts of sodium and aluminum entering the structure of quartz and the intimate intergrowth texture of the run products may contribute to the ob- served pressure shift. Combined petrological and mineralogical studies on the run products and the natural rocks yield the fol- lowing prograde reaction sequence to have occurred： The protolith of the jadeite- quartzite from Dabie Mountain is an albitized siltstone/greywacke characterized by an albite＋quartz assemblage. During prograde metamorphism albite breaks down to form jadeite＋quartz and thus at this stage two types of quartz can be distinguished whereas type-I-quartz already existed in the pro- tolith, type-II-quartz represents a newly formed reaction product of albite. During further P-T-increase the pure type- I-quartz was transformed to coesite, whereas type-II-quartz （together with jadeite） was still present as a stable phase because of its im- purities of Na and A1. At a later stage during further subduction, type-II-quartz also decomposes to form coesite. These studies represent an important puzzlement for a better understanding of the evolution of jadeite- quartzite from the Dabie Mountain during continental crust subduction and thus contribute to a more complete knowledge of the formation of the Dabie Mountain UHP orogenic belt in general.展开更多
文摘Small granitic intrusions occur in the progressive metamorphic belts of the Chinese Ahai orogen. SHRIMP U-Pb analyses were performed on zircons separated from a tonalite intrusion and yielded a concordant age of 409.6±3.7 Ma （ MSWD = 0.93 ）, restricting the emplacement and crystallization of the tonalite intru- sion to the Early Devonian. Combined with the existing geological data of the contemporary large granitic plutons in the Chinese Altai orogen, the tonalite is considered to be formed together with other granitic rocks in a continental arc setting. The tonalite intrusion has consistent foliation with its country rocks, indicating the strain resuiting in the regional deformation should be very strong during or after the early Devonian.
基金supported by the Research Projects of China(Grants Nos.2009CB825003,41002068)the State Key Laboratory of GPMR(Grant No.MSF-GPMR 200911)China University of Geosciences(Grant No.CUGL090204)
文摘Jadeite quartzite, essentially a two-phase rock made up of jadeite and quartz, is one of the most important UHP lithologies occur- ring in the Dabie Mountain ultrahigh pressure metamorphic belt and forms layers in biotite-plagioclase gneiss. High pressure- high temperature studies on natural albite from the country rock gneiss were undertaken to reveal the--in parts----complex mineralogical changes that occur in the jadeite quartzite during prograde metamorphism. Experiments were conducted at 800- 1200~C, in the pressure range of 2.0-3.5 GPa. One of the most intriguing results shows that the low pressure boundary of the jadeite＋coesite stability field is located between about 3.2 GPa at 1000~C and 3.4 GPa at 1200~C, thus about （0.2-0.3）_＋0.1 GPa higher than the quartz-coesite transition curve, given the uncertainty in the present study. Minor amounts of sodium and aluminum entering the structure of quartz and the intimate intergrowth texture of the run products may contribute to the ob- served pressure shift. Combined petrological and mineralogical studies on the run products and the natural rocks yield the fol- lowing prograde reaction sequence to have occurred： The protolith of the jadeite- quartzite from Dabie Mountain is an albitized siltstone/greywacke characterized by an albite＋quartz assemblage. During prograde metamorphism albite breaks down to form jadeite＋quartz and thus at this stage two types of quartz can be distinguished whereas type-I-quartz already existed in the pro- tolith, type-II-quartz represents a newly formed reaction product of albite. During further P-T-increase the pure type- I-quartz was transformed to coesite, whereas type-II-quartz （together with jadeite） was still present as a stable phase because of its im- purities of Na and A1. At a later stage during further subduction, type-II-quartz also decomposes to form coesite. These studies represent an important puzzlement for a better understanding of the evolution of jadeite- quartzite from the Dabie Mountain during continental crust subduction and thus contribute to a more complete knowledge of the formation of the Dabie Mountain UHP orogenic belt in general.
